An algorithm for rapid computation of the steady-state thermal structure of mature subduction zones. - J. Alcock (Comput. Geosci., 2005)

One- and two-dimensional models are equally effective in monitoring the crust's thermal response to advection by large-scale thrusting during orogenesis. - J. Alcock; José R. Martínez Catalán; R. Arenas (Comput. Geosci., 2011)